Fig 6 - uploaded by Ioan I Bucur
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Calcareous algae. a-c, f Salpingoporella muehlbergii (Lorenz); a, longitudinal section, thin section RR4835; b, longitudinal-slightly oblique, and transverse sections; thin section RR4838; c, f oblique sections; thin sections RR4839 (c) and RR4838 (f). d, e Salpingoporella cf. muehlbergii (Lorenz); thin RR4839 (d) and RR4840(e). g Salpingoporella muehlbergii (Lorenz) (Sm) oblique section, and foraminifer trocholinid (T); thin section RR4836. h Similiclypeina aff. somalica Conrad, Peybernès & Masse (Ss) longitudinal section, and Salpingoporella muehlbergii (Lorenz) (Sm) transverse section; thin section RR4835. i Salpingoporella muehlbergii (Lorenz) (Sm) transverse section, and Similiclypeina conradi Bucur (Sc) transverse-oblique section; thin section RR4835. j Salpingoporella muehlbergii (Lorenz) (Sm) oblique section, and Sporolithon rude (Lemoine) (Sr); thin section RR4839. k Arabicodium sp.; thin section RR4834. Scale bar is 0.25 mm.
Source publication
An exploratory borehole cross-cutting Miocene deposits near Derezna (south of Kučevo town, Eastern Serbia) has intercepted Lower Cretaceous carbonate rocks in its lower part. The identified microfacies and micropaleontological associations indicate a Barremian age for these limestones. Among the identified dasycladalean algae, Salpingoporella patru...
Contexts in source publication
Context 1
... dominated by muddy facies (wackestone, wackestone-packstone or packstone) and subordinate packstone-grainstone or coarse grainstone (Fig. 4a-h (Fig. 7a), Korkyrella texana Sokač (Fig. 7b, c), Salpingoporella biokovensis Sokač & Velić (Fig. 7d), Clypeina div. sp. (Fig. 7e-h), Actinoporella podolica (Alth) [Fig. 7i, j, l, m (Ap)], Arabicodium? sp. (Fig. 6k ...
Context 2
... foraminifera are less frequent. They are represented by: Mayncina sp. (Fig. 8a), Banatia aninensis Schlagintweit & Bucur (Fig. 8b, c), Moulladella jourdanensis (Foury & Moullade) (Fig. 8d), small textulariaceans, miliolids and trocholinids [ Fig. 6g ...
Context 3
... helvetica Morellet & Morellet, 1918 from Eocene (cf. Schlagintweit et al., 2013); see also Clypeina in Genot, 1980;2009, andin Granier & Lethier, 2019). By contrast, Heteroporella? paucicalcarea presents a compact skeleton since its whorls are welded in their vertical succession (see for instance the detached specimens in Bucur, 2011, pl. 1, fig. 6). As a consequence, the generic affiliation of these controversial species still remains ...
Context 4
... dominated by muddy facies (wackestone, wackestone-packstone or packstone) and subordinate packstone-grainstone or coarse grainstone (Fig. 4a-h (Fig. 7a), Korkyrella texana Sokač (Fig. 7b, c), Salpingoporella biokovensis Sokač & Velić (Fig. 7d), Clypeina div. sp. (Fig. 7e-h), Actinoporella podolica (Alth) [Fig. 7i, j, l, m (Ap)], Arabicodium? sp. (Fig. 6k ...
Context 5
... foraminifera are less frequent. They are represented by: Mayncina sp. (Fig. 8a), Banatia aninensis Schlagintweit & Bucur (Fig. 8b, c), Moulladella jourdanensis (Foury & Moullade) (Fig. 8d), small textulariaceans, miliolids and trocholinids [ Fig. 6g ...
Context 6
... helvetica Morellet & Morellet, 1918 from Eocene (cf. Schlagintweit et al., 2013); see also Clypeina in Genot, 1980;2009, andin Granier & Lethier, 2019). By contrast, Heteroporella? paucicalcarea presents a compact skeleton since its whorls are welded in their vertical succession (see for instance the detached specimens in Bucur, 2011, pl. 1, fig. 6). As a consequence, the generic affiliation of these controversial species still remains ...
Context 7
... dominated by muddy facies (wackestone, wackestone-packstone or packstone) and subordinate packstone-grainstone or coarse grainstone (Fig. 4a-h (Fig. 7a), Korkyrella texana Sokač (Fig. 7b, c), Salpingoporella biokovensis Sokač & Velić (Fig. 7d), Clypeina div. sp. (Fig. 7e-h), Actinoporella podolica (Alth) [Fig. 7i, j, l, m (Ap)], Arabicodium? sp. (Fig. 6k ...
Context 8
... foraminifera are less frequent. They are represented by: Mayncina sp. (Fig. 8a), Banatia aninensis Schlagintweit & Bucur (Fig. 8b, c), Moulladella jourdanensis (Foury & Moullade) (Fig. 8d), small textulariaceans, miliolids and trocholinids [ Fig. 6g ...
Context 9
... helvetica Morellet & Morellet, 1918 from Eocene (cf. Schlagintweit et al., 2013); see also Clypeina in Genot, 1980;2009, andin Granier & Lethier, 2019). By contrast, Heteroporella? paucicalcarea presents a compact skeleton since its whorls are welded in their vertical succession (see for instance the detached specimens in Bucur, 2011, pl. 1, fig. 6). As a consequence, the generic affiliation of these controversial species still remains ...
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Citations
A mixed assemblage of planktonic and benthonic foraminifera (e.g. orbitolinids) is reported from proximal calciturbidites within the ‘Lower Flyschoid Formation’ of the western part of the Slovenian Basin. The presence of reworked orbitolinids from the Slovenian territory is well known, but their treatment in open nomenclature has hitherto hindered biostratigraphic analyses. The onset of sedimentation of the Lower Flyschoid Formation was previously indicated as Albian and possibly Aptian. The records of Palorbitolina lenticularis (Blumenbach) and Mesorbitolina gr. lotzei Schroeder tibetica (Cotter) at the base of the formation, which overlies the Biancone Limestone with an erosional contact indicates the presence of uppermost lower Aptian reworking in some places. The presence of Conicorbitolina cuvillieri (Moullade) in the upper parts of the studied sections indicates a late Albian-early Cenomanian age. The ages obtained from the neritic faunal elements is generally in line with the data obtained from the associated planktonic foraminifera. C. cuvillieri characterizes platform margin and upper slope deposits, with very few records in the literature. From the wider area, it has been recorded from the northernmost part of the Dinaric-Friuli Carbonate Platform of Italy and Slovenia thus allowing for platform-to-basin as well as inter-basinal correlations. The youngest age obtained from the Lower Flyschoid Formation is middle Cenomanian. The new data indicate a diachronous base of the Lower Flyschoid Formation needing further investigations for deciphering the palaeogeographic configuration at the northwestern edge of the Friuli Carbonate Platform as well as platform events in relationship to contemporaneous basinal sequences.
